Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 3
Poor snowpack structure remains, and it has proven capable of producing large, destructive human-triggered avalanches. The likelihood of triggering one of these avalanches is decreasing, but the consequences remain severe. Any avalanche failing on the PWL will take out the entire season’s snowpack and will instantly be a season-ender, or worse. The weak layer of concern is right below the Christmas rain crust. In some locations, this crust may temporarily support the weight of a skier or rider, but its ability to bridge underlying weaknesses is highly variable and unreliable. The most dangerous slopes are above treeline and face north and east, especially those that harbor a more robust slab from previous wind loading.
I will approach this situation by biting off small pieces of avalanche terrain. I’ll be looking for slopes with no steep convexities, terrain traps, thin rocky areas or slab margins, and clean runouts. This problem can be avoided altogether by sticking to slopes less steep than 30 degrees.